Plate Boundaries-Divergent-Convergent-Transform - MooMooMath and Science (360p, h264, youtube)
Plate Boundaries
Overview
Dramatic changes in the Earth's crust occur along plate boundaries, including:
Formation of mountain ranges
Creation of new islands
Occurrence of earthquakes
There are three main types of plate boundaries:
Divergent Boundaries
Convergent Boundaries
Transform Boundaries
Convergent Boundaries
Occur when two tectonic plates collide.
Types of Convergent Boundaries:
Continental to Continental
Two plates of continental crust collide.
Results in buckling and thickening of the crust, forming mountains.
Continental to Oceanic
Ocean crust collides with continental crust.
Oceanic crust, being thicker, subducts under the continental crust.
Resultant magma from melted oceanic crust leads to the formation of volcanoes along the boundary.
Ocean to Ocean
When two plates of oceanic crust collide.
The older, denser plate subducts under the younger plate.
This melting results in the creation of an island arc.
Divergent Boundaries
Occur when two plates move away from each other.
Separation allows the asthenosphere (soft layer of the mantle) to rise towards the surface and partially melt.
This melting creates magma that erupts as lava.
Lava cools and hardens to create new rock, forming new ocean floor or continental crust.
Formation of new lithosphere occurs as the upper part of the asthenosphere cools and becomes rigid.
Often found on the ocean floor, but can also create rift valleys when continents are separated.
Transform Boundaries
Occur where two plates move past each other horizontally.
The movement is not smooth; plates scrape against each other causing sudden slippages of crustal rock, which can be felt as earthquakes.
Unlike convergent and divergent boundaries, transform boundaries typically do not produce magma.
Example: San Andreas Fault in California is a major transform boundary.
Conclusion
Recap of the three types of plate boundaries:
Convergent
Divergent
Transform
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